Geophysical crews have been collecting seismic data on the Arctic Coastal Plain for over 40 years. Most work is performed during the winter months to avoid environmental damage to the tundra. Seismic crews routinely operate over frozen lakes as well as on first year sea ice, and data collection may begin as soon as the ice is strong enough to support the equipment. Traditionally, the safe-bearing capacity of ice has been related to a minimum thickness and a subjective determination of the condition of the ice. This criterion has been established through years of experience and, for the most part, it has been quite successful. Ice conditions are monitored throughout the winter by drilling at designated intervals. This results in accurate thickness data at the collection points but does not provide any information between the points. Ice thickness by itself is not a good indication of ice strength. It is possible to have an ice sheet that is several feet thick and have near zero strength. However, flexural strength may be estimated when ice profiles are used in conjunction with other data. In an effort to obtain continuous profiles of the ice-water interface, a series of ground-penetrating radar (GPR) tests were performed. A GPR system was tested on lake ice as well as sea ice. In both cases, the bottom of the ice could be imaged. Radar profiles are normally displayed on a time scale. To convert the time scale to ice thickness, it is necessary to calculate the relative permittivity of the ice sheet. This is easily accomplished in the field. First year sea ice is a very complex mixture of ice, brine, and air. As the surface temperature of sea ice drops below freezing, small disks and needles of pure ice, termed frazil ice, form on the surface …